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physical geology lecture test # 2 - summer 2010
physical geology lecture test # 2 - summer 2010

... 53. Chemical sedimentary structures are formed ? deposition. A.before B.during C.after 54. ? may be used to determine ancient current direction. A.nodules B.geodes C.concretions D.migmatites E.cross-bedding ...
INSIDE EARTH: CHAPTER 3
INSIDE EARTH: CHAPTER 3

... There are about 600 active volcanoes on land. Many more lie below the sea.  Ring of Fire:a major volcanic belt formed by many volcanoes at the rim of the Pacific Ocean  Most volcanoes occur along diverging plate boundaries, such as the mid-ocean ridge or in subduction zones around the edges of oce ...
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PTYS/ASTR 206 – Section 2 - Lunar and Planetary Laboratory
PTYS/ASTR 206 – Section 2 - Lunar and Planetary Laboratory

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Year 9 Term 1: Earth and Space- Plate Tectonics 2015 (Week 6-10)
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Twentieth lecture - 23 October, 2013
Twentieth lecture - 23 October, 2013

... Individual reworked zircons in NW Australia have been dated to 4.3 BILLION yrs. ...
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Plate Tectonics

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Plate Tectonics - Boone County Schools
Plate Tectonics - Boone County Schools

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Plate Tectonics Unit Assessment Study Guide Answers

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(comprised of the continental crust and oceanic crust).
(comprised of the continental crust and oceanic crust).

... comprised of a number of concentric layers. At the center is the core (a solid inner core and a liquid outer core). Surrounding the core is the mantle (similar to mafic minerals like olivine and the ultramafic peridotite). The outer most layer is the crust (comprised of the continental crust and oce ...
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Composition of the earth, Geologic Time, and Plate Tectonics
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... Crust (earth): The outer shell of the earth comprising oceanic and continental components with a specific gravity of 2.6-2.65. Convergent boundary: The leading edge of an advancing continental margin. Usually associated with subduction, deformation and volcanism. Daughter product: A nuclide formed b ...
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... • A. by the shape and size of the rock sample • B. by how quickly the molten magma cooled • C. by the place in the world the sample was found. • D. by whether there are layers or bands ...
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Convergent Boundaries - Colliding Plates

...  The crust is forced deep into the earth where high _________ and _________ cause trapped water and other gases to be released. This, in turn, makes the base of the crust melt, forming _____________.  The magma formed rises up toward the earth’s surface and builds up in _____________ _____________ ...
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... During the early 1960s, seismologists studying earthquake seismic waves detected the layer configuration of the Earth’s crust, mantle, outer and inner core. They found that the crust and the upper most portion of the mantle actually acted together as a single brittle layer. They called this the lith ...
Geo rev 1 (intro)
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How did plate tectonics emerge on Earth?

... lithosphere to form and join up, and thus make up plate boundaries, according to a model proposed by two geophysicists, Yanick Ricard from the Laboratoire de Géologie de Lyon (CNRS/Université Claude Bernard Lyon 1/ENS de Lyon) and his colleague David Bercovici (Yale University, US). The model assume ...
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Alfred Wegener 1880-1930
Alfred Wegener 1880-1930

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Plate Tectonics Links together 2 theories

... how the Earth evolved over time. ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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